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脱硫石膏与谷氨酸副产物协同改良旱塬土壤及增加玉米产量

Synergistic improvement of dryland soil and maize yield by combined application of flue gas desulfurization gypsum and glutamic acid by-products

  • 摘要: 针对旱塬区土壤水分短缺、养分瘠薄及水肥利用效率低等问题,本研究旨在探究脱硫石膏与谷氨酸复配改良剂提升土壤水肥特性和玉米产量的适配性及作用机制,以期为旱塬区玉米绿色生产与土壤质量提升旱地农业的高效绿色发展提供理论参考与技术借鉴。在山西省晋中市设置田间小区试验,共设7个处理:不施改良剂(CK)、改良剂Ⅰ号(60%脱硫石膏+40%谷氨酸渣)和改良剂Ⅱ号(60%脱硫石膏+40%谷氨酸液)均设置3个施用量水平,分别为7.5、15.0和22.5 t/hm2。测定收获期0~20 cm土层土壤水肥特性、离子组成及玉米产量,结合随机森林模型识别影响产量的关键因子。结果表明:1)改良剂Ⅱ号各用量均显著提高了土壤含水量(P<0.05),增幅为22.9%~30.3%,而改良剂Ⅰ号仅在高用量(22.5 t/hm2)下效果显著(增幅25.6%,P<0.05)。2)两种改良剂均显著降低了土壤pH,其中改良剂Ⅰ号降幅(0.5~0.7个单位)略大于Ⅱ号(0.3~0.7个单位),同时土壤电导率因水溶性Ca2+、Mg2+、SO42-等浓度增加而显著上升,且随施用量增加呈递增趋势。3)土壤有机碳、碱解氮和有效磷含量均显著提高(P<0.05),其中改良剂Ⅱ号对有机碳和碱解氮的提升作用明显,而改良剂Ⅰ号对有效磷的活化效果更为突出。4)玉米产量随改良剂用量增加而提高,改良剂Ⅰ号的最高增产效应(47.0%)优于Ⅱ号(30.1%),随机森林模型显示土壤电导率、碱解氮、SO42-、Ca2+、有机碳、有效磷、速效钾和Mg2+是影响产量的关键因子。综上,改良剂Ⅰ号(22.5 t/hm2)可通过协同改善土壤水盐状况、提升养分有效性实现最优改土增产效果,在晋中旱塬区及类似生态区的具有潜在应用前景。

     

    Abstract: A tradeoff is often required between soil reclamation and crop productivity in sustainable agriculture. However, the critical constraints have caused soil water scarcity, nutrient impoverishment, and low hydro-thermal-nutrient use efficiency in the dryland loess regions of Northern China. This study aimed to evaluate the synergistic soil improvement via the combined application of flue gas desulfurization (FGD) gypsum and glutamic acid fermentation by-products (residue and liquid). This study aims to provide theoretical references and technical support for the green productionof maizae in dry plateau areas, the improvement of soil quality, and the efficient and green development of dryland agriculture. A systematic plot experiment was conducted in the maize field of Jinzhong dryland region, Shanxi Province, China, during an extremely arid growing season in 2024. Seven treatments included: a control (CK, without amendment), and two composite amendments at three rates (7.5, 15.0, and 22.5 t/hm2). Amendment I was formulated with 60% FGDG and 40% glutamic acid liquid, while Amendment II consisted of 60% FGD gypsum and 40% glutamic acid liquid. The parameters were then determined at the harvest stage, including key soil parameters in the 0–20 cm layer, water-soluble ion compositions, and maize agronomic traits. The results demonstrated that both composite amendments exerted significant modulating effects on soil water-salt-nutrient dynamics. In terms of hydrological properties, Amendment-II exhibited a highly stable water retention (P<0.05), with the soil water content increasing by 22.9% to 30.3% among all dosages, whereas Amendment-I shared a significant effect (25.6% increase, P<0.05) only at the highest rate (22.5 t/hm2). Furthermore, both amendments significantly mitigated alkalinity (P<0.05) in soil reaction, thus reducing pH values by 0.3 to 0.7 units. Specifically, Amendment-I treatment demonstrated a superior acidification potential (0.5–0.7 unit reduction), due to its lower raw pH (2.51) and higher residual acidity. Concurrently, soil electrical conductivity (EC) increased from a baseline of 134 μS/cm to the range of 235.0%–461.0% (Amendment-I) and 115.0%–320.0% (Amendment-II), compared with the CK. This EC enhancement was primarily attributed to the substantial input of beneficial water-soluble ions. Among them, Ca2+ concentrations increased by 314.3%–757.1% (Amendment-I), while SO42- concentrations were 18.5 to 56.0 times those in the CK. Nutrient availability was enhanced by the synergistic mechanisms of inorganic structural improvement and organic fertility supplementation. Amendment-II shared more pronounced effects on soil organic carbon (SOC) and alkali-hydrolyzable nitrogen (AN), with the increments of 47.8%–56.0% and 17.4%–26.7%, respectively. Conversely, Amendment I enhanced 113.2%–252.0% of available phosphorus (AP) in the CK, likely due to the localized dissolution of mineral phosphates and the chelation of organic acids in the fermentation residue. Maize grain yield responded dose-dependently to amendment application. Amendment I achieved the maximum yield increment of 47.0%, thereby outperforming the 30.1% increase recorded for Amendment II. Random Forest modeling was implemented to identify soil EC, with the AN, SO42-, Ca2+, SOC, AP, AK, and Mg2+ as the most influential factors for the maize yield. The EC contributed the most, with the highest relative importance (14.6%). The input of secondary-element cations (Ca2+ and Mg2+) and anions (SO42-) also served a nutritional and stress-resilience role rather than inducing salinity stress under the nutrient-limited conditions of dryland degradation. Agronomically, yield improvements were attributed largely to hundred-grain weight (up to 24.5% increase) and ear diameter, indicating optimal source-sink dynamics during the grain filling stage. In conclusion, the optimal strategy was taken as the synergetic application of Amendment-I at a rate of 22.5 t/hm2 for soil reclamation and yield enhancement in the dryland region. While substantial short-term benefits occurred under extreme drought conditions, multi-year fixed-site monitoring was essential to evaluate the long-term environmental safety, salt accumulation kinetics, and the potential bioaccumulation of trace heavy metals. This finding can provide a scientific basis for the high-value utilization of industrial by-products in dryland agriculture.

     

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